Form Number F Ratio Classifier
Constituent form ratio(K1+O1)/(M2+S2) with caller independently chosen inclusive tidal-class edges, no table inference. Caller independently establishes units, regime, calibration and applicability; this does not establish design-code compliance, authenticity, operational safety, treatment efficacy or a validated forecast.
Description
A tidal form number compares diurnal with semidiurnal constituent amplitudes.
A tidal form number compares diurnal with semidiurnal constituent amplitudes.1
Classification can use supplied inclusive upper edges rather than an assumed universal label table.
When to use Form Number F Ratio Classifier
Use this tool to calculate or review the supplied observations under the stated rules. Match the observation interval, units, datum, coordinate signs and model regime.
How to use Form Number F Ratio Classifier and understand its results
- Match the observation interval, units, datum, coordinate signs and model regime.
- Enter k1AmplitudeM, o1AmplitudeM, m2AmplitudeM, s2AmplitudeM, callerInclusiveFormClassUpper, using the field meanings and rules below, then run the tool.
- Read tidalFormNumber, callerFormClassIndex. Inspect nested result fields where present, and review unknown records separately from known matches.
- Correct any reported input issue and run again. Before using a successful result, check the stated units, signs, reference scope and observation coverage.
| Input field | Meaning | Value type | Requirement |
|---|---|---|---|
| k1AmplitudeM | K1 amplitude m | number | Required |
| o1AmplitudeM | O1 amplitude m | number | Required |
| m2AmplitudeM | M2 amplitude m | number | Required |
| s2AmplitudeM | S2 amplitude m | number | Required |
| callerInclusiveFormClassUpper | Caller inclusive form class upper | list of number | Required |
All four amplitudes must be nonnegative and M2+S2 positive. Require a nonempty strictly increasing nonnegative upper-edge list. Return (K1+O1)/(M2+S2) and the zero-based first edge containing it inclusively, or the list length for the overflow class.
F=(K1+O1)/(M2+S2); index=first j with F≤upper_j, else edgeCount Use the matching field units and the exact boundary, ordering and reference rules above.
| Output field | Meaning | Value type |
|---|---|---|
| tidalFormNumber | Tidal form number | number |
| callerFormClassIndex | Caller form class index | number |
{
"input": {
"k1AmplitudeM": 1,
"o1AmplitudeM": 2,
"m2AmplitudeM": 2,
"s2AmplitudeM": 1,
"callerInclusiveFormClassUpper": [
0.25,
1.5,
3
]
},
"output": {
"tidalFormNumber": 1,
"callerFormClassIndex": 1
}
} Limitations and assumptions
The stated observation or model covers only the supplied record and reference regime. It does not fill missing measurements, supply uncertainty estimates or produce a validated forecast.
Missing required fields, unknown fields, wrong types and violated rules return input issues. Numeric values and outputs must be finite. Lists and matrices must be dense, without missing cells. Numeric lists allow at most 10000 entries; ordinary string lists allow at most 128 strings of 128 UTF-16 units each; numeric matrices allow at most 128 rows and 128 columns, subject to narrower requirements above.
Alternative or Complementary methods
For a related step, use Estuarine Circulation Ratio UE Calculator: An estuarine circulation ratio compares surface flow with residual flow over a matched section. For a complementary comparison, use Equilibrium Tide Theoretical Amplitude Calculator: Equilibrium tide height relates a constituent’s tide-generating potential to gravity.
References
-
Form Number F Ratio Classifier — tool.io
Similar or alternative tools
- Estuarine Circulation Ratio UE Calculator
An estuarine circulation ratio compares surface flow with residual flow over a matched section.
- Equilibrium Tide Theoretical Amplitude Calculator
Equilibrium tide height relates a constituent’s tide-generating potential to gravity.